If this sounds familiar, there’s a good chance you’ve witnessed a USGS Hydrologic Technician in action, making an ice discharge measurement. For most Minnesotan’s, venturing onto river ice is a one-way ticket to Valhalla, but for the intrepid streamgager, navigating river ice is routine work! "Why are they out there, you might say?" Well, because the USGS calculates streamflow year around, even when the river is frozen over.
In Minnesota, ice typically sets in around late November, a celebrated time known to many mid-westerners as “Ice-In”.
Ice discharge measurements play a crucial role in estimating the winter portion of annual hydrographs. Each year as rivers begin to freeze over, backwater becomes the rule, not the exception. This backwater affect refers to the fluctuations in gage height caused by the formation and release of channel ice. During these periods, the typical stage-discharge relations used to calculate discharge become unreliable.
Much like summer open water wading measurements, Winter ice measurements utilize similar methods for measuring area and velocity used in the computation of stream flow. The key difference lies in the need to drill through the ice to measure the flowing water beneath. A minor inconvenience, but well worth the effort.
Ice measurements can be safe and successful with the right approach. The trick is knowing when to walk away from a dangerous situation. Even the most seasoned streamgager can be fooled by the capricious nature of river ice. To avoid risk, the USGS streamgager is equipped to test the ice ahead of each step. This precaution helps avoid the perils of treading on thin ice. For a streamgager, a sturdy chisel in hand and some good common sense is your best friend.
As the seasons shift from summer to winter, USGS streamgagers begin their preparations for making annual ice measurements. They bring out their sleds, sharpen their chisels, fuel their ice augers, and dust off those lime green float coats that can be seen by distant passerby’s.
You might ask, “is there really a difference between an ice measurement and a summer wading measurement?” And the streamgager might reply, with a hint of mirth " the proof is in the footing!"